Smoke radiocarbon measurements from Indonesian fires provide evidence for burning of millennia-aged peat.

Autor: Wiggins EB; Department of Earth System Science, University of California, Irvine, CA 92697; elizabeth.b.wiggins@nasa.gov jranders@uci.edu., Czimczik CI; Department of Earth System Science, University of California, Irvine, CA 92697., Santos GM; Department of Earth System Science, University of California, Irvine, CA 92697., Chen Y; Department of Earth System Science, University of California, Irvine, CA 92697., Xu X; Department of Earth System Science, University of California, Irvine, CA 92697., Holden SR; Department of Earth System Science, University of California, Irvine, CA 92697., Randerson JT; Department of Earth System Science, University of California, Irvine, CA 92697; elizabeth.b.wiggins@nasa.gov jranders@uci.edu., Harvey CF; Center for Environmental Sensing and Modeling, Singapore-MIT Alliance for Research and Technology, 138602 Singapore.; Parsons Laboratory, Department of Civil and Environmental Engineering, Massachusetts Institute of Technology, Cambridge, MA, 02139., Kai FM; Center for Environmental Sensing and Modeling, Singapore-MIT Alliance for Research and Technology, 138602 Singapore., Yu LE; Department of Civil & Environmental Engineering, National University of Singapore, 119260 Singapore.; National University of Singapore Environmental Research Institute, National University of Singapore, 119260 Singapore.
Jazyk: angličtina
Zdroj: Proceedings of the National Academy of Sciences of the United States of America [Proc Natl Acad Sci U S A] 2018 Dec 04; Vol. 115 (49), pp. 12419-12424. Date of Electronic Publication: 2018 Nov 19.
DOI: 10.1073/pnas.1806003115
Abstrakt: In response to a strong El Niño, fires in Indonesia during September and October 2015 released a large amount of carbon dioxide and created a massive regional smoke cloud that severely degraded air quality in many urban centers across Southeast Asia. Although several lines of evidence indicate that peat burning was a dominant contributor to emissions in the region, El Niñ o -induced drought is also known to increase deforestation fires and agricultural waste burning in plantations. As a result, uncertainties remain with respect to partitioning emissions among different ecosystem and fire types. Here we measured the radiocarbon content ( 14 C) of carbonaceous aerosol samples collected in Singapore from September 2014 through October 2015, with the aim of identifying the age and origin of fire-emitted fine particulate matter (particulate matter with an aerodynamic diameter less than or equal to 2.5 μm). The Δ 14 C of fire-emitted aerosol was -76 ± 51‰, corresponding to a carbon pool of combusted organic matter with a mean turnover time of 800 ± 420 y. Our observations indicated that smoke plumes reaching Singapore originated primarily from peat burning (∼85%), and not from deforestation fires or waste burning. Atmospheric transport modeling confirmed that fires in Sumatra and Borneo were dominant contributors to elevated PM 2.5 in Singapore during the fire season. The mean age of the carbonaceous aerosol, which predates the Industrial Revolution, highlights the importance of improving peatland fire management during future El Niño events for meeting climate mitigation and air quality commitments.
Competing Interests: Conflict of interest statement: S.E.P. and C.F.H. are coauthors on a 2017 letter to the editor.
(Copyright © 2018 the Author(s). Published by PNAS.)
Databáze: MEDLINE